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avg atomic mass
avg atomic mass = the sum of each isotope mass times its abundance
diatomic elements
H, N, Fl, O, Cl, I, Br
finding empirical formula and molecular formula from % composition
turn %s into g (assume sample is 100g)
find mols of each element
divide by smallest number of mols
round to nearest integer
divide mass of molecular compound by mass of empirical formula to find factor of each element
equations where one reactant is in excess
find how many mols of each reactant
find possible mass of product from limiting reactant
find how much of the other reactant is needed for that product
subtract that mass from total mass of excess reactant to find unreacted mass
% yield
% yield = actual yield / theoretical yield
determining MM of unknown reactant
calculate mols of product
calculate proportionate mols of reactant
divide mass of reactant by mols
Solubility Rules
Soluble - alkali metals, ammonium, (NO3)-, (CH3CO2)-, Cl/Br/I
not with Cu+, Ag+, Pb 2+
Insoluble - (OH)-, (S) 2-, (CO3)2-, (PO4)3-, (SO4)2- with a main group cation
not with, alkali metal, NH4, alkali earth metal, Mg2+ or 2+ transition metal
Strong Acids - break apart and ionize, high conductivity, covalent
HCl, HBr, HI, HNO3, HClO4, H2SO4
Strong Base - break apart and ionize, high conductivity, ionic
LiOH, NaOH, KOH, Ca(OH)2, Sr(OH)2, Ba(OH)2
Electrolytes - conduct electricity
Strong - soluble compounds, strong acids/bases, ions
Weak - weak acids/bases
non-electrolyte - insoluble compound
Oxidation Numbers
element in naturally occurring form: 0
charged monatomic ions: their charge
commands: sum of ox# = 0
oxygen: -2
hydrogen: +1
halogens: -1
OIL RIG
if ox# increase, electrons are lost, species is oxidized, reducing agent
if ox# decrease, electrons are gained, species is reduced, oxidizing agent
types of reactions
precipitation (forms a solid)
acid-base (reactants are an acid and a base)
neutralization
gas formation
oxidation reduction (elements change ox#)
combustion
single displacement
dilution equation
M1V1 = M2V2
conversions
1kcal = 4.184 kJ
0 C = 273.15 K
energy and enthalpy equations
KE = 0.5mv² (kg, m/s)
Δ𝐸=𝑤+𝑞 (kJ)
internal energy = work + heat
work done by system and heat released will be negative
w=-pΔV (atm, L)
work = -(pressure) (change in volume)
𝑞=𝑚𝑐Δ𝑇 (J or cal, g, C or K) *c and T units must match
heat absorbed/released = (mass)(specific heat capacity)(change in temp)
specific heat of water = 4.184
path vs state functions
path - depends on how system got from one state to another
heat, work
state - depends only on current state of system
T, P, V, ΔE, ΔH
calculate ΔHrxn by manipulating equations
multiply and divide, or flip equations so that products and reactants cancel
add enthalpies
calculate ΔHrxn from Hf
find the enthalpy of formation of each species from chart
products - reactants
IMFs
Intermolecular
London Dispersion
Dipole-Dipole
H-Bonding (hydrogen must be bonded to NOF, other NOF must have lone pair)
Intramolecular
covalent
metallic
ionic
ideal gas law
PV=nRT
(atm, L, mol, 0.0821, K)
combined gas law
(P1V1/n1T1) = (P2V2/n2T2)
density and mass equations
MM = mRT/PV
MM= dRT/P
partial pressures
the total pressure of a gaseous mixture is equal to the sum of the partial pressures
diffusion vs effusion
diffusion - gases move through space until they’ve mixed completely
effusion - gases move through a small pinhole
properties of substances with strong IMFs
high boiling point
low vapor pressure
high surface tension
high viscosity
phase diagram
triple point - all three phases can exist at once
critical point - distinction between gas and liquid is lost
spontaneous reaction
displacement reaction will occur if lone cation is move reactive than cation in compound